Grilli R, Marrocco N, Desbois T, Guillerm C, Triest J, Kerstel E, Romanini D
CNRS, LIPhy, F-38000 Grenoble, France.
DT INSU CNRS, Bât. IPEV BP 74, Technopole Brest Iroise, 29280 Plouzané, France.
Rev Sci Instrum. 2014 Nov;85(11):111301. doi: 10.1063/1.4901018.
This article describes the advances made in the development of a specific optical spectrometer based on the Optical Feedback-Cavity Enhanced Absorption Spectroscopy technique for exploring past climate by probing the original composition of the atmosphere stored in the ice sheet of a glacier. Based on significant technological progresses and unconventional approaches, SUBGLACIOR will be a revolutionary tool for ice-core research: the optical spectrometer, directly embedded in the drilling probe, will provide in situ real-time measurements of deuterium isotopic variations (δ(2)H ) and CH4 concentrations down to 3500 m of ice depth within a single Antarctic season. The instrument will provide simultaneous and real-time vertical profiles of these two key climate signatures in order to evaluate if a target site can offer ice cores as old as 1.5 million years by providing direct insight into past temperatures and climate cycles. The spectrometer has a noise equivalent absorption coefficient of 2.8 × 10(-10) cm(-1) Hz(-1/2), corresponding to a detection limit of 0.2 ppbv for CH4 and a precision of 0.2‰ on the δ(2)H of H2O within 1 min acquisition time.
本文介绍了一种基于光反馈腔增强吸收光谱技术的特定光学光谱仪在开发过程中取得的进展,该光谱仪用于通过探测冰川冰盖中储存的大气原始成分来探索过去的气候。基于重大的技术进步和非常规方法,SUBGLACIOR将成为冰芯研究的革命性工具:直接嵌入钻探探头的光学光谱仪将在单个南极季节内提供冰深达3500米处氘同位素变化(δ(2)H)和CH4浓度的原位实时测量。该仪器将提供这两个关键气候特征的同步实时垂直剖面,以便通过直接洞察过去的温度和气候周期来评估目标地点是否能提供长达150万年的冰芯。该光谱仪的噪声等效吸收系数为2.8×10(-10) cm(-1) Hz(-1/2),在1分钟采集时间内,对应CH4的检测限为0.2 ppbv,H2O的δ(2)H精度为0.2‰。